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The serpulid tube worms from the Eocene deposits of Soh and Zefreh in Central Iran and their palaeoecological implication

This study reports the first findings of *Rotularia leptostoma* and *Ditrupa strangulata* in Eocene deposits of central Iran, providing new insights into their microstructure, palaeoecology, and the marine currents linking Europe and North America during that period.

Original authors: Tomáš Kočí, Martina Kočová Veselská, Ali Bahrami, Mehdi Yazdi, Arash Mohammad Rezaei, Lenka Váchová, Rok Gašparič

Published 2026-10-06
📖 5 min read🧠 Deep dive

Original authors: Tomáš Kočí, Martina Kočová Veselská, Ali Bahrami, Mehdi Yazdi, Arash Mohammad Rezaei, Lenka Váchová, Rok Gašparič

Original paper licensed under CC BY 4.0 (https://creativecommons.org/licenses/by/4.0/). ✨ This is an AI-generated explanation of the paper below. It is not written or endorsed by the authors. For technical accuracy, refer to the original paper. Read full disclaimer

Deep beneath the waves of ancient seas, long before humans walked the earth, a different kind of architect was at work. These were not builders of stone or wood, but tiny marine worms that secreted hard, calcium-based tubes to protect their soft bodies. Known as serpulids, these tube-dwelling creatures are a common sight in the fossil record, often found cemented to rocks or shells. However, a specific group of these worms, including the genera Rotularia and Ditrupa, developed a unique strategy. Instead of attaching themselves to a hard surface, they lived freely on the soft, shifting mud of the ocean floor. To survive in this unstable environment, they evolved heavy, coiled tubes with sharp ridges or keels that acted like ballast, keeping them upright and preventing them from sinking into the sediment. By studying the fossilized remains of these worms, scientists can reconstruct the ancient environments they inhabited, understanding everything from water depth and temperature to the strength of ocean currents and the stability of the sea floor.

In a recent study, researchers turned their attention to the Eocene deposits of central Iran, specifically the regions around Soh and Zefreh. For years, the only known serpulid from this part of Iran was a single species of Rotularia. However, a new investigation has uncovered a much richer and more diverse community. The team collected hundreds of specimens from limestone and marl layers dating back to the middle Eocene. Among the finds were dozens of specimens of Rotularia spirulaea, a species previously known from Europe and North America, and the first-ever records of two other species in Iran: Rotularia leptostoma and Ditrupa strangulata. The sheer abundance of these worms in the rock layers suggests they were a dominant part of the local ecosystem, living alongside other marine life such as large single-celled organisms called foraminifera, various snails, clams, and even ancient crabs.

To understand exactly what these creatures were and how they lived, the researchers did more than just count and measure the fossils. They took a closer look at the microscopic structure of the tube walls. Using powerful microscopes, they examined the tiny crystals that make up the calcium carbonate of the tubes. They found that the different species had distinct internal architectures. For instance, the tube of Ditrupa strangulata is built from two layers: an outer layer with a ridged, prism-like pattern and an inner layer that is fine and grainy. In contrast, Rotularia leptostoma has a more complex three-layered wall, with a thin inner layer, a middle layer of irregular crystals, and an outer layer of short, semi-ordered crystals. These microscopic details are crucial because they allow scientists to distinguish between species that might look almost identical to the naked eye, confirming that the Iranian fossils represent specific, identifiable species rather than just generic worm tubes.

The study also revealed evidence of life-and-death struggles in this ancient sea. On two specimens of Rotularia leptostoma, the researchers found small, circular holes drilled into the shell. These holes were shallow and incomplete, suggesting that a predator, likely a snail, attempted to drill through the tube to reach the worm inside but failed. These marks, known as drill holes, provide a rare glimpse into the predatory interactions of the time, showing that even these small, soft-bottom dwellers were part of a complex food web. The fact that the holes were not fully penetrated indicates that the worm either survived the attack or that the predator gave up, perhaps because the tube was too thick or the worm too well-protected.

Beyond the worms themselves, the fossils tell a story about the geography and climate of the region. The presence of these specific worms, along with the types of shells and microscopic organisms found with them, points to a warm, shallow marine environment. The sediment layers, which alternate between fine mud and coarser sand, suggest that the sea floor was subject to periodic high-energy events, such as strong currents or storms, which stirred up the bottom. The worms found here were well-adapted to these conditions; their heavy, keeled tubes allowed them to remain stable on the soft, shifting mud even when the water was turbulent. This contrasts with other fossil sites in Iran where different types of worms lived attached to hard surfaces, suggesting that the Soh and Zefreh areas were distinct environments, perhaps slightly deeper or more prone to sediment movement than their neighbors.

The discovery also helps map the ancient connections between continents. The species found in Iran, particularly Rotularia leptostoma, are also known from the Eocene rocks of Texas, Austria, and Germany. This wide distribution suggests that these worms were excellent travelers, capable of moving across vast ocean distances. The researchers propose that these creatures likely migrated between Europe and North America via the Atlantic Ocean, following the warm currents of the time, rather than traveling across the Pacific. The presence of these same species in Iran, situated on the ancient Tethys Sea, supports the idea of a connected marine world where life could spread freely across what are now separate continents. By piecing together the microscopic details of these tiny tubes, the researchers have not only identified new species for Iran but also painted a clearer picture of the dynamic, interconnected ocean world that existed millions of years ago.

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